Geological Bulletin, Volume 12University of Peshawar, 1979 - Geology |
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Page 14
It is also observed that the carbonate minerals are more prominant in the basal
part as compared to the upper part. However, no gradual change is observed.
Recrystallization of the carbonate minerals is also an important textural feature ...
It is also observed that the carbonate minerals are more prominant in the basal
part as compared to the upper part. However, no gradual change is observed.
Recrystallization of the carbonate minerals is also an important textural feature ...
Page 17
The view is further confirmed by the fact that glauconite is present only in the very
basal part of the formation. Ore minerals Ore minerals are present in a minor
amount in the basal part but dominate the upper part and the shaly intercalations.
The view is further confirmed by the fact that glauconite is present only in the very
basal part of the formation. Ore minerals Ore minerals are present in a minor
amount in the basal part but dominate the upper part and the shaly intercalations.
Page 25
Traces of glauconite and a few ghost structures are noticed in the very basal part
of the formation. They are observed at levels containing little calcareous minerals
. Since they are absent from the rest of the formation, the writers suggest that ...
Traces of glauconite and a few ghost structures are noticed in the very basal part
of the formation. They are observed at levels containing little calcareous minerals
. Since they are absent from the rest of the formation, the writers suggest that ...
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Contents
and the Baghanwala Formation | 1 |
Khewra Gorge Khewra Jehlutn District | 11 |
Mineral Poliey with special reference | 41 |
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Common terms and phrases
anhedral Baghanwala Formation basal basin biotite calcarenite calcareous cement calcilutite texture calcisiltite texture calcite Cambrian carbonate and limonite carbonate matrix carbonate minerals Cementing material characterized by calcarenite chlorite clayey cement colour Compactibility corroded boundaries cross-bedding cubic pseudomorphs deposition detrital Dolomitic limestone environments feldspar fossils freely circulated Geology of India Ghundai Sar glauconite granoblastic highly corroded indicate interbeddings intercalations iron oxide iron oxide pigmentation Jehlum KHAN Khewra Gorge Khussak Formation Khyber Agency laminated layers less corroded long shore currents marine water maroon material is carbonate metamorphism mica micaceous mineral sector Minerals are anhedral mud cracks Muscovite non-clastic observed Pakistan Peshawar PETROGRAPHY Plagioclase porosity pseudomorphs Punjab quartz quartz grains recrystallized ripple marks rock texture salt crystals Salt Range sandstone sedimentary rocks sedimentary structures sediments shale siltstone slides stable shelf area strata stratification stratigraphic stratigraphic levels stylolites texture is metamorphic thin bedded Thin Section Tobra Formation underlying Jutana Dolomite Univ upper worm burrows